Neural criticality from effective latent variables

Observations of power laws in neural activity data have raised the intriguing notion that brains may operate in a critical state. One example of this critical state is “avalanche criticality,” which has been observed in various systems, including cultured neurons, zebrafish, rodent cortex, and human EEG. More recently, power laws were also observed in neural populations in the mouse under an activity coarse-graining procedure, and they were explained as a consequence of the neural activity being coupled to multiple latent dynamical variables. An intriguing possibility is that avalanche criticality emerges due to a similar mechanism. Here, we determine the conditions under which latent dynamical variables give rise to avalanche criticality. We find that populations coupled to multiple latent variables produce critical behavior across a broader parameter range than those coupled to a single, quasi-static latent variable, but in both cases, avalanche criticality is observed without fine-tuning of model parameters. We identify two regimes of avalanches, both critical but differing in the amount of information carried about the latent variable. Our results suggest that avalanche criticality arises in neural systems in which activity is effectively modeled as a population driven by a few dynamical variables and these variables can be inferred from the population activity.


Introduction
The neural criticality hypothesis -the idea that neural systems operate close to a phase transition, perhaps for optimal information processing -is both ambitious and banal.Measurements from biological systems are limited in the range of spatial and temporal scales that can be sampled, not only because of the limitations of recording techniques but also due to the fundamentally nonstationary behavior of most, if not all, biological systems.These limitations make proving that an observation indicates critical behavior difficult.At the same time, the idea that brain networks are critical echoes the anthropic principle: tuned another way, a network becomes quiescent or epileptic and in either state, seems unlikely to support perception, thought, or flexible behavior, yet these observations do not explain how such fine-tuning could be achieved.Further muddying the water, researchers have reported multiple kinds of criticality in neural networks, including through analysis of avalanches (Beggs and Plenz, 2003;Plenz et al., 2021;O'Byrne and Jerbi, 2022;Girardi-Schappo, 2021) and of coarse-grained activity (Meshulam et al., 2019), as well as of correlations (Dahmen et al., 2019).How these flavors of critical behavior relate to each other or any functional network mechanism is unknown.
The phenomenon that we will refer to as "avalanche criticality" appears remarkably widespread.It was first observed in cultured neurons (Beggs and Plenz, 2003) and later studied in zebrafish (Ponce-Alvarez et al., 2018), turtles (Shew et al., 2015), rodents (Ma et al., 2019), monkeys (Peter-1 of 23 arXiv:2301.00759v3[q-bio.NC] 13 Oct 2023Oct mann et al., 2009)), and even humans (Poil et al., 2008).The standard analysis, described later, requires extracting power-law exponents from fits to the distributions of avalanche size and of duration and assessing the relationship between exponents.There is debate over whether these observations reflect true power laws, but within the resolution achievable from experiments, neural avalanches exhibit power laws with exponent relationships predicted from theory developed in physical systems (Perković et al., 1995).
Avalanche criticality is not the only form of criticality observed in neural systems.Zipf's law, in which the frequency of a network state is inversely proportional to its rank, appears in systems as diverse as fly motion estimation and the salamander retina (Mora and Bialek, 2010;Schwab et al., 2014;Aitchison et al., 2016).More recently, Meshulam et al. (2019) reported various statistics of population activity in the mouse hippocampus, including the eigenvalue spectrum of the covariance matrix and the activity variance.These were found to scale as populations were "coarsegrained" through a procedure in which neural activities were iteratively combined based on similarity.Similar observations have been reported in spontaneous activity recorded across a wide range of brain areas in the mouse (Morales et al., 2023).Simple neural network models of such data explain neither Zipf's law nor coarse-grained criticality (Meshulam et al., 2019).
Even though these three forms of criticality are observed through different analyses, they may originate from similar mechanisms.Numerous studies have reported relatively low-dimensional structure in the activity of large populations of neurons (Mazor and Laurent, 2005;Ahrens et al., 2012;Mante et al., 2013;Pandarinath et al., 2018;Stringer et al., 2019;Nieh et al., 2021), which can be modeled by a population of neurons that are broadly and heterogeneously coupled to multiple latent (i.e., unobserved) dynamical variables.Using such a model, we previously reproduced scaling under coarse-graining analysis within experimental uncertainty (Morrell et al., 2021).Zipf's law has been explained by a similar mechanism (Schwab et al., 2014;Aitchison et al., 2016;Humplik and Tkačik, 2017).A single quasi-static latent variable has been shown to produce avalanche power laws, but not the relationships expected between the critical exponents (Priesemann and Shriki, 2018), while a model including a global modulation of activity can generate avalanche criticality (Mariani et al., 2021), but has not demonstrated coarse-grained criticality (Morrell et al., 2021).It is not known under what conditions the more general latent dynamical variable model generates avalanche criticality.
Here we examine avalanche criticality in the latent dynamical variable model of neural population activity.We find that avalanche criticality is observed over a wide range of parameters, some of which may be optimal for information representation.These results demonstrate how criticality in neural recordings can arise from latent dynamics in neural activity, without need for fine-tuning of network parameters.

Critical exponents values and crackling noise
We begin by defining the metrics used to quantify avalanche statistics and briefly summarize experimental observations, which have been reviewed in detail elsewhere (Plenz et al., 2021;O'Byrne and Jerbi, 2022;Girardi-Schappo, 2021).Activity is recorded across a set of neurons and binned in time.Avalanches are then defined as contiguous time bins, in which at least one neuron in the population is active.The duration of an avalanche is the number of contiguous time bins and the size is the summed activity during the avalanche.The distributions of avalanche size and duration are fit to power laws ( () ∼  − for size , and  () ∼  − for duration ) using standard methods (Clauset et al., 2009).
Power laws can be indicative of criticality, but they can also result from non-critical mechanisms (Touboul and Destexhe, 2017;Priesemann and Shriki, 2018).A more stringent test of criticality is the "crackling" relationship (Perković et al., 1995;Touboul and Destexhe, 2017), which involves fitting a third power-law relationship, S() ∼   fit , and comparing  fit to the predicted exponent  pred , derived from the size and duration exponents,  and : Previous work demonstrating approximate power laws in size and duration distributions through the mechanism of a slowly changing latent variable did not generate crackling (Touboul and Destexhe, 2017;Priesemann and Shriki, 2018).
Measuring power-laws in empirical data is challenging: it generally requires setting a lower cutoff in the size and duration, and the power-law behavior only has limited range due to the finite size and duration of the recording itself.Nonetheless, there is some consensus (Shew et al., 2015;Fontenele et al., 2019;Ma et al., 2019) that even if  and  vary over a wide range (1.5 to about 3) across recordings, the values of  fit and  pred stay in a relatively narrow range, from about 1.1 to 1.3.

Avalanche scaling in a latent dynamical variable model
We study a model of a population of neurons that are not coupled to each other directly but are driven by a small number of latent dynamical variables -that is, slowly changing inputs that are not themselves measured (Fig. 1A).We are agnostic as to the origin of these inputs: they may be externally driven from other brain areas, or they may arise from large fluctuations in local recurrent dynamics.The model was chosen for its simplicity, and because we have previously shown that this model with at least about five latent variables can produce power laws under the coarse-graining analysis (Morrell et al., 2021).In this paper, we examine avalanche criticality in the same model.
Specifically, we model the neurons as binary units (  ) that are randomly (  ∼ (0, 1)) coupled to dynamical variables ℎ  ().The probability of any pattern {  }, given the current state of the latent variables, is where the parameter  controls the scaling of the variables and  controls the overall activity level.
We modeled each latent variable as an Ornstein-Uhlenbeck process with the time scale   (see Methods).Thus our model has four parameters:  (input scaling),  (activity threshold),   (dynamical timescale), and   (number of latent variables).Distributions of avalanche size and avalanche duration within this model followed approximate power laws (Fig. 1C; see Methods).In the example shown (  = 5,   = 10 4 ,  = 4 and  = 12), we found exponents  = 1.89 ± 0.02 (size) and  = 2.11 ± 0.02 (duration).Further, the average size of avalanches with fixed duration scaled as  ∼   , with the fitted  fit = 1.24 ± 0.02, in agreement with the predicted value  pred = 1.24±0.02.Thus, our model could generate avalanche scaling, at least for some parameter choices.In the following sections, we examine how avalanche scaling depends on model parameters (  ,   ,  and ; see Table 2).We first focus on two sets of simulations: one set with   = 1 latent variable, which does not generate scaling under coarse-graining (Morrell et al., 2021), and one set with   = 5 latent variables, which can generate such scaling for some values of parameters   , , and  (Morrell et al., 2021).

Avalanche scaling depends on the number of latent variables
We analyzed avalanches from one-and five-variable simulations, each with fixed latent dynamical timescale (  = 5 × 10 3 time steps; see Table 2 for parameters).In the following sections, time is measured in simulation time steps, see Methods for converting time steps to seconds.We used established methods for measuring empirical power laws (Clauset et al., 2009).The minimum cutoffs for size ( min ) and duration ( min ) are indicated by vertical lines in Fig. 2. For the population coupled to a single latent variable, the avalanche size distribution was not well fit by a power law (Fig. 2A).With a sufficiently high minimum cut-off ( min ), the duration distribution was approximately powerlaw (Fig. 2B).2. A-C: Scaling analysis for one variable models where the dynamic timescale is equal to 5 × 10 3 time steps.A: Distribution of avalanche sizes.MLE value of exponent for best-fit power law is  = 1.98 (0.02 SE), with lower cutoff indicated by the vertical line.B: Distribution of avalanche duration.MLE value of  is 1.81 (0.02 SE).C: Average size plotted against avalanche duration (blue points), with power-law fit (black line) and predicted relationship (yellow line) from MLE values for exponents in A and B. Gray bar on the horizontal axis indicates range, over which a power law with  = 1.72 fits the data (see Methods).D-F: Analysis of avalanches from a simulation of a population coupled to five independent latent variables where the dynamic timescale is equal to 5 × 10 3 time steps.G: Exponents  for avalanche size distributions across timescales for one-variable (blue) and five-variable (red) simulations.Each circle is a simulation with independently drawn coupling parameters.Simulations had to show scaling over at least two decades to be included in panels (G-J).H: Exponents  for avalanche duration distributions for simulations in G. I: Fitted values of  for simulations in G. J: Difference between fitted and predicted  values.Five-variable simulations produce crackling over a wider range of timescales than single-variable simulations.We next assessed whether the simulation produced crackling.If so, the value  fit obtained by fitting S() ∼   fit would be similar to  pred = −1 −1 .In many cases, such as the one-variable example shown in Fig. 2C, the full range of avalanche durations were not fit by a single power law.Therefore, we determined the largest range, over which a power law was a good fit to the simulated observations.In this case, slightly over two decades of apparent scaling were observed starting from avalanches with minimum duration slightly less than 100 time steps (Fig. 2C), with a best-fit value of    ∈ [1.69, 1.74].As we did not find a power-law in the size distribution, calculating  pred is meaningless.If we do it anyway, we obtain   = 0.83 ± 0.03 (yellow line in Fig. 2C), which clearly deviates from the fitted value of .Thus, for the single latent dynamical variable model (  = 5000), power-law fits are poor, and there is no crackling.
The five-variable model produces a different picture.We now find avalanches, for which size and duration distributions are much better fit by power-law models starting from very low minimum cutoffs (Fig. 2D-E, Fig. 2-Supp.Fig. 2).Average size scaled with duration, again over more than two decades, with  f it = 1.27 ± 0.03, which was in close agreement with  pred = 1.25 ± 0.02 (Fig. 2F).Holding other parameters constant, we thus found that scaling relationships and crackling arise in the multi-variable model but not the single-variable model.

Avalanche scaling depends on the time scale of latent variables
Based on simulations in the previous section, we surmised that the five-variable simulation generated scaling more readily due to creating an "effective" latent variable that had slower dynamics than any individual latent variable.We reasoned that at any moment in time, the latent variable state ℎ  () is a vector in the latent space.Because coupling to the latent variables is random throughout the population, only the length (∼ √   ) and not the direction of this vector matters, and the timescale of changes in this length would be much slower than   , the timescale of each of the components ℎ  ().We therefore speculated that increasing the timescale of dynamics of the latent variables should eventually lead to scaling and crackling in the single-variable model as well as the five-variable one.To examine the dependence of avalanche scaling on this timescale, we simulated one-variable and five-variable networks at fixed  and  coupled to latent variables with the correlation time of their Ornstein-Uhlenbeck dynamics of   ∈ [10 3 , 10 5 ] time steps, spanning from a factor of 10 faster to a factor of 10 slower than the original   in Fig. 1.Simulations were replicated five times at each combination of parameters by drawing new latent variable coupling values (  ), as well as new latent variable dynamics and instances of neural firing.For simulations that passed the criteria to be fitted by power laws, we plot the fitted values of  , ,  fit and  fit −  pred (Fig. 2G-J).Missing points are those, for which distributions did not pass the power law fit criteria.
In the single-variable model, best-fit exponents changed abruptly for latent variable timescale around   = 10 4 (Fig. 2G, H), while in the five-variable model, exponents tended to increase gradually (Fig. 2G, H, red).The discontinuity in the single-variable case reflected a change in the lower cutoff values in the power-law fits: size and duration distributions generated with faster latent dynamics could be fit reasonably well to a power law by using a high value of the lower cutoff (Fig. 2-Supp.Fig. 3).For time scales greater than ∼ 10 4 , the minimum cutoffs dropped, and the single-variable model generated power-law distributed avalanches and crackling (Fig. 2J), similar to the five-variable model.In summary, in the latent dynamical variable model, introducing multiple variables generated scaling at faster timescales.However, by slowing the timescale of the latent dynamics, the model generated signatures of critical avalanche scaling for both multi-and single-variable simulations.

Avalanche criticality, input scaling, and firing threshold
In the previous section, we found that a very slow single latent dynamical variable generated avalanche criticality in the simulation population.Thus, from now on, we simplify the model in order to characterize avalanche statistics across values of input scaling  and firing threshold .Specifically, we modeled a population of  = 128 neurons coupled to a single quasi-static latent variable.We simulated 10 3 segments of 10 4 steps each and drew a new value of the latent variable (ℎ ∼ (0, 1)) for each segment.Ten replicates of the simulation were generated at each of the combinations of  and  (see Methods).
Almost independent of  and , we found quality power law fits and crackling.Fig. 3 shows the average (across  = 10 network realizations) of the exponents extracted from size (, Fig. 3A) and duration (, Fig. 3C) distributions.At small firing threshold ( = 2), we do not observe scaling because the system is always active, and all avalanches merge into one.At large firing threshold  and low input scaling , we do not observe scaling because activity is so sparse that all avalanches are small.At intermediate values of the parameters, the simulations generated plausible scaling relationships in size and duration.The difference between  fit and  pred was typically less than 0.1 (Fig. 4D-F), which was consistent with previously reported differences between fit and predicted exponents (Ma et al., 2019).Thus, there appears to be no need for fine-tuning to generate apparent scaling in this model, at least in the limit of (near) infinite observation time.Wherever  and  generate avalanches, there are approximate power-law distributions and crackling.
To determine where avalanches occur, we derive the avalanche rate across values of the latent variable ℎ.In the quasi-static model, the probability of an avalanche initiation is the probability of a transition from the quiet to an active state.Because all neurons are conditionally independent, this is  ava =  silence (1 −  silence ).Then the expected number of avalanches Nava is obtained by integrating  ava over ℎ at each value of  and : where (ℎ) is the standard normal distribution.This probability tracks the observed number of avalanches across simulations, Fig. 4A.
To gain an intuition for the conditions, under which avalanches occur, we show two slices of the avalanche probability, at fixed  (Fig. 4B) and at fixed  (Fig. 4C).Black regions indicate where avalanches are likely to occur.If, for a given value of  and , there is no overlap between high avalanche probability regions and the distribution of ℎ, then there will be no avalanches.For large , avalanches occur because neurons with large coupling to the latent variable (|  | >> 1, recall   ∼ (0, 1)) are occasionally activated by a value of the latent variable ℎ that is sufficient to exceed  (Fig. 4B).Thus, the scaling parameter  controls the value of ℎ, for which avalanches occur most frequently (Fig. 4C).As  decreases, avalanches occur for smaller and smaller ℎ until avalanches primarily occur when ℎ = 0.
To calculate the probability of avalanches, we must integrate over all values of ℎ, but we can gain a qualitative understanding of which avalanche regime the system is in by examining the probability of avalanches at ℎ = 0.At ℎ = 0, the avalanche probability (see Methods) is which is maximized at  0 = − log(2 1∕ − 1), independent of   and .After some algebra, we find that  0 ∼ log  for large .The dependence on  reflects that a larger threshold is required for larger networks: large networks ( → ∞) are unlikely to achieve complete network silence, therefore preventing avalanches from occurring.Similarly, small networks ( ∼ 1) are unlikely to fire consecutively and thus are unlikely to avalanche.We plot  ava (, ;   , , ℎ = 0) as a function of  in Fig. 4D.The peak at  0 divides the space into two regions.For  <  0 , a power-law is only observed in the large-size avalanches, which are rare (Fig. 4E, green).By contrast, when  >  0 , minimum size cutoffs are low (Fig. 4F, orange).Both regions,  <  0 and  >  0 , exhibit crackling noise scaling.If observation times are not sufficiently long (estimated in Fig. 4-Supp.Fig. 1), then scaling will not be observed in the  <  0 region, whose scaling relations consist of rare events.Insufficient observation times may explain experiments and simulations where avalanche scaling was not found.

Inferring the latent variable
Our analysis of  ava (, , ℎ) at ℎ = 0 suggested that there are two types of avalanche regimes: one with high activity and high minimum cutoffs in the power law fit (Type 1), and the other with lower activity and size cutoffs (Type 2).Further, when  ava drops to zero, avalanches disappear because the activity is too high or too low.We now examine how information about the value of the latent variables represented in the network activity relates to the activity type.To delineate these types, we calculated numerically  * (), the value of , for which the probability of avalanches is maximized, and the contours of  ava (Fig. 5A).Curves for  * () and  0 and  ava = 10 −3 are shown in Fig. 5A and B.
We expect that the more cells fire, the more information they would convey, until the firing rate saturates, and inferring the value of the latent variable becomes impossible.Fig. 5B supports the prediction: generally, information is higher in regions with more activity (lower , higher ), but only up to a limit: as  → 0, information decreases.This decrease begins approximately where the probability of avalanches drops to nearly zero (dashed black lines, Fig. 5B-E) because all of  the activity merges into a few very large avalanches.In other words, the Type-1 avalanche region coincides with the highest information about the latent variable.
The critical brain hypothesis suggests that the brain operates in a critical state, and its functional role may be in optimizing information processing (Beggs, 2008;Chialvo, 2010).Under this hypothesis, we would expect the information conveyed by the network to be maximized in the regions we observe avalanche criticality.However, we see that critical regions do not always have optimal information transmission.In Fig. 5, the region that displays crackling noise is that where avalanches exist ( ava > 0.001), which corresponds to any  value and  ≳ 3.This avalanche region encompasses both networks with high information transmission and networks with low information transmission.In summary, observing avalanche criticality in a system does not imply a high-information processing network state.However, the scaling can be seen at smaller cutoffs, and hence with shorter recordings, in the high-information state.This parallels the discussion by Schwab et al. (2014), who noticed that the Zipf's law always emerges in neural populations driven by quasi-stationary latent fields, but it emerges at smaller system sizes when the information about the latent variable is high.

Discussion
Here we studied systems with distributed, random coupling to latent dynamical variables and we found that avalanche criticality is nearly always observed, with no fine-tuning required.Avalanche criticality was surprisingly robust to changes in input gain and firing rate threshold.Loss of avalanche criticality could occur if the latent process was not well-sampled, either because the simulation was not long enough or the dynamics of the latent variables were too fast.Finally, while information about the latent variables in the network activity was higher where avalanches were generated compared to when they were not, there was a range of information values across the critical avalanche regime.Thus, avalanche criticality alone was not a predictor of optimal information transmission.

Explaining experimental exponents
A wide range of critical exponents has been found in ex vivo and in vivo recordings from various systems.For instance, the seminal work on avalanche statistics in cultured neuronal networks by Beggs and Plenz (2003) found size and duration exponents of 1.5 and 2.0 respectively, along with  = 2, when time was discretized with a time bin equal to the average inter-event interval in the system.A subset of the in vivo recordings analyzed from anesthetized cat (Hahn et al., 2010) and macaque monkeys (Petermann et al., 2009) also exhibited a size distribution exponent close to 1.5.By contrast, a survey of many in vivo and ex vivo recordings found power-law size distributions with exponents ranging from 1 to 3 depending on the system (Fontenele et al., 2019).Separately, Ma et al. (2019) reported recordings in freely moving rats with size exponents ranging from 1.5 to 2.7.In these recordings, when the crackling relationship held, the reported value of  was near 1.2 (Fontenele et al., 2019;Ma et al., 2019).
A model for generating avalanche criticality is a critical branching process (Beggs and Plenz, 2003), which predicts size and duration exponents of 1.5 and 2 and scaling exponent  of 2. However, there are alternatives: Lombardi et al. (2023) showed that avalanche criticality may also be produced by an adaptive Ising model in the sub-critical regime, and in this case, the scaling exponent  was not 2 but close to 1.6.Our model, across the parameters we tested that produced exponents consistent with the scaling relationship, generated  values that ranged from 1.9 to about 2.5.Across those simulations, we found values  within a narrow band from 1.1 to 1.3 (see Fig. 2I, J and Fig. 3H).While the exponent values our model produces are inconsistent with a critical branching process ( = 2), they match the ranges of exponents estimated from experiments and reported by Fontenele et al. (2019).In this context, it might be useful to explore if our model and that of Lombardi et al. (2023) might be related, with the adaptive feedback signal of the latter viewed as an effective, latent variable of the former.
A genuine challenge in comparing exponents estimated from different experiments with different recording modalities (spiking activity, calcium imaging, LFP, EEG, or MEG) arises from differences in spatial and temporal scale specific to a particular recording, as well as the myriad decisions made in avalanche analysis, such as defining thresholds or binning in time.Thus, one possible reason for differences in exponents across studies may derive from how the system is sub-sampled in space or coarse-grained in time, both of which systematically change exponents  and  (Beggs and Plenz, 2003;Shew et al., 2015) and could account for differences in  (Capek et al., 2023).The model we presented here could be used as a test bed for examining how specific analysis choices affect exponents estimated from recordings.
A second possible explanation for differences in exponents is that different experiments study similar, but distinct biological phenomena.For instance, networks that were cultured in vitro may differ from those that were not, whether they are in vivo or ex vivo (i.e., brain slices), and sensoryprocessing networks may have different dynamics from networks with different processing demands.It is possible that certain networks develop connections between neurons such that they truly do produce dynamics that approximate a critical branching process, while other networks have different structure and resulting dynamics and thus can be better understood as coupled neurons receiving feedback (Lombardi et al., 2023) or as a system coupled to latent dynamical variables.This is especially true in sensory systems, where coupling to (latent) external stimuli in a way that the neural activity can be used to infer the stimuli is the reason for the networks' existence (Schwab et al., 2014).

Relationship to past modeling work
Our model is not the first to produce approximate power-law size and duration distributions for avalanches from a latent variable process (Touboul and Destexhe, 2017;Priesemann and Shriki, 2018).In particular, Priesemann and Shriki (2018) derived the conditions, under which an inhomogeneous Poisson process could produce such approximate scaling.The basic idea is to generate a weighted sum of exponentially distributed event sizes, each of which are generated from a homogeneous Poisson process.How each process is weighted in this sum determines the approximate power-law exponent, allowing one to tune the system to obtain the critical values of 1.5 and 2. Interestingly, this model did not generate non-trivial scaling of size with duration ( ∼   ).Instead, they found  = 1, not the predicted  = 2. Our results differ significantly, in that  was typically between 1.1 and 1.3 and it was nearly always close to the prediction from  and .We speculate that this is due to nonlinearity in the mapping from latent variable to spiking activity, as doubling the latent field ℎ does not double the population activity, but doubling the rate of a homogeneous Poisson process does double the expected spike count.As biological networks are likely to have such nonlinearities in their responses to common inputs, this scenario may be more applicable to certain kinds of recordings.

Summary
Latent variables -whether they are emergent from network dynamics (Clark et al., 2022;Sederberg and Nemenman, 2020) or derived from shared inputs -are ubiquitous in large-scale neural population recordings.This fact is reflected most directly in the relatively low-dimensional structure in large-scale population recordings (Stringer et al., 2019;Pandarinath et al., 2018;Nieh et al., 2021).We previously used a model based on this observation to examine signatures of neural criticality under a coarse-graining analysis and found that coarse-grained criticality is generated by systems driven by many latent variables (Morrell et al., 2021).Here we showed that the same model also generates avalanche criticality, and that when information about the latent variables can be inferred from the network, avalanche criticality is also observed.Crucially, finding signatures of avalanche criticality required long observation times, such that the latent variable was well-sampled.Previous studies showed that Zipf's law appears generically in systems coupled to a latent variable that changes slowly relative to the sampling time, and that the Zipf's behavior is easier to observe in the higher information regime (Schwab et al., 2014;Aitchison et al., 2016).However, this also suggests that observation of either scaling at modest data set sizes indeed points to some fine-tuning -namely to the increase of the information in the individual neurons (and, since neurons in these models are conditionally independent, also in the entire network) about the value of the latent variables.In other words, one would expect a sensory part of the brain, if adapted to the statistics of the external stimuli, to exhibit all of these critical signatures at relatively modest data set sizes.In monocular deprivation experiments, when the activity in the visual cortex is transiently not adapted to its inputs, scaling disappears, at least for recordings of a typical duration, and is restored as the system adapts to the new stimulus (Ma et al., 2019).We speculate that the observed recovery of criticality by Ma et al. (2019) could be driven by neurons adapting to the reduced stimuli state, for instance, by adjusting  (input scaling) and  (firing rate threshold).
Taken together, these results suggest that critical behavior in neural systems -whether based on the Zipf's law, avalanches, or coarse-graining analysis -is expected whenever neural recordings exhibit some latent structure in population dynamics and this latent structure can be inferred from observations of the population activity.

Simulation of Dynamic Latent Variable model
We study a model from Morrell et al. (2021), originally constructed as a model of large populations of neurons in mouse hippocampus.In the original version of the model, neurons are noninteracting, receiving inputs reflective of place-field selectivity as well as input current arising from a random projection from a small number of latent dynamical variables, representing inputs shared across the population of neurons that are not directly measured or controlled.In the current pa-per, we incorporate only the latent variables (no place variables), and we assume that every cell is coupled to every latent variable with some randomly drawn coupling strength.
The probability of observing a certain population state {  } given latent variables ℎ  () at time  is where  is the normalization, and  is the "energy": The latent variables ℎ  () are Ornstein-Uhlenbeck processes with zero mean, unit variance, and time constant   .Couplings   are drawn from the standard normal distribution.
Parameters for each figure are laid out in Tables 1-3.For the infinite time constant simulation, we draw a value ℎ  ∼  (0, 1) and simulate for 10000 time steps, then repeat for 1000 draws of ℎ  .

Time step units
Most results were presented using arbitrary time units: all times (i.e.,   and avalanche duration ) are measured in units of an unspecified time step.Specifying a time bin converts the probability of firing into actual firing rates, in spikes per second, and this choice determines which part of the - phase space is most relevant to a given experiment.The time step is the temporal resolution at which activity is discretized, which varies from several to hundreds of milliseconds across different experimental studies (Beggs and Plenz, 2003;Fontenele et al., 2019;Ma et al., 2019).In physical units and assuming a bin size of 3 ms to 10 ms, our choice of  and  in Fig. 2 would yield physiologically realistic firing rate ranges (Hengen et al., 2016), with high-firing neurons reaching averages rates of 20 − 50 spikes/second and median firingrate neurons around 1 − 2 spikes/second.The timescales of latent variables examined range from about 3 seconds to 3000 seconds, assuming 3-ms bins.Inputs with such timescales may arise from external sources, such as sensory stimuli, or from internal sources, such as changes in physiological state.
Simulations were carried out for the same number of time steps (2 × 10 6 ), which would be approximately 1 to 2 "hours," which is a reasonable duration for in vivo neural recordings.Note that at large values of   , the latent variable space is not well sampled during this time period.

Analysis of avalanche statistics
Setting the threshold for observing avalanches In our model, we count avalanches as periods of continuous activity (in any subset of neurons) that is book-ended by time bins with no activity in the entire simulated neural network.For real neural populations of modest size, this method fails because there are no periods of quiescence.The typical solution is to set a threshold, and to only count avalanches when the population activity exceeds that threshold, with the hope that results are relatively robust to that choice.In our model, this operation is equivalent to changing , which shifts the probability of firing up or down by a constant amount across all cells independent of inputs.Our results in Fig. 3 show that  and  decrease as the threshold for detection is increased (equivalent to large ||), but that the scaling relationship is maintained.The model predicts that  pred −  f it would initially increase slightly with the detection threshold before decreasing back to near zero.
Following the algorithm laid out in Clauset et al. (2009), we fit power laws to the size and duration distributions from simulations generating avalanches.We use least-squares fitting to estimate  f it , the scaling exponent for size with duration, assessing the consistency of the fit across decades.

Reading power laws from data
We want, from each simulation, a quantification of the quality of scaling (how many decades, minimally) and an estimate of the scaling exponents ( for the size distribution,  for the duration distribution).We first compile all avalanches observed in the simulation and for each avalanche, calculate its size (total activity across the population during the avalanche) and its duration (number of time bins).Following the steps outlined by Clauset et al. (2009), we use the maximum-likelihood estimator to determine the scaling exponent.This is the solution to the transcendental equation where (,  min ) is the Hurwitz zeta function and   are observations; that is, either the size or the duration of each avalanche .For values of  min < 6, a numerical look-up table based on the built-in Hurwitz zeta function in the symbolic math toolbox was used (MATLAB2019b).For  min > 6 we use an approximation (Clauset et al. (2009)), To determine  min , we computed the maximum absolute difference between the empirical cumulative density (()) function and model's cumulative density function  () (the Kolmogorov-Smirnov (KS) statistic;  = max ≥ min |()− ()|).The KS statistic was computed between for powerlaw models with scaling parameter α and cutoffs  min .The value of  min that minimizes the KS statistic was chosen.Occasionally the KS statistic had two local minima (as in Figure 2-Supplemental Figure 1), indicating two different power-laws.In these cases, the minimum size and duration cutoffs were the smallest values that were within 10% of the absolute minimum of the KS statistic.
Note that the statistic is computed for each model only on the power-law portion of the CDF (i.e. ≥  min ).We do not attempt to determine an upper cut-off value.
To assess the quality of the power-law fit, Clauset et al. (2009) compared the empirical observations to surrogate data generated from a semi-parametric power-law model.The semi-parametric model sets the value of the CDF equal to the empirical CDF values up to  =  min and then according to the power-law model for  >  min .If the KS statistic for the real data (relative to its fitted model) is within the distribution of the KS statistics for surrogate datasets relative to their respective fitted models, the power-law model was considered a reasonable fit.
Strict application of this methodology could give misleading results.Much of this is due to the loss of statistical power when the minimum cutoff is so high that the number of observations drops.For instance, in the simulations shown in Fig. 2, the one-variable duration distribution passed the Clauset et al. (2009) criterion, with a minimum KS statistic of 0.03 when the duration cutoff was 18 time steps.However, for the five-variable simulation in Fig. 2, a power-law would be narrowly rejected for both size and duration, despite having much smaller KS statistics: for , the KS statistic was 0.0087 (simulation range: 0.0008 to 0.0082; number of avalanches observed: 58, 787) and for  it was 0.0084 (simulation range: 0.0011 to 0.0075).Below we discuss this problem in more detail.
Determining range, over which avalanche size scales with duration For fitting , our aim was to find the longest sampled range, over which we have apparent powerlaw scaling of size with duration.Because our sampled duration values have linear spacing, error estimates are skewed if a naive goodness of fit criterion is used.We devised the following algorithm.First, the simulation must have at least one avalanche of size 500.We fit  =   over one decade at a time.We chose as the lower duration cutoff the value of minimum duration, for which the largest number of subsequent (longer-duration) fits produced consistent fit parameters (Figure 2-Supp.Fig. 3 and 4, top row).Next, with the minimum duration set, we gradually increased the maximum duration cut-off, and we determined whether there was a significant bias in the residual over the first decade of the fit.We selected the highest duration cutoff, for which there was no bias.Finally, over this range, we re-fit the power law relationship and extracted confidence intervals.
Our analysis focused on finding the apparent power-law relationship that held over the largest log-scale range.A common feature across simulation parameters (  ,   ) was the existence of two distinct power-law regimes.This is apparent in Fig. 2I, which shows that when   = 1 at small   , the best-fit  (that showing the largest range with power-law-consistent scaling) is much larger (> 1.7), and then above   ∼ 3000, the best-fit  drops to around 1.3.

Statistical power of power-law tests
In several cases, we found examples of power-law fits that passed the rejection criteria commonly used to determine avalanche scaling relationships because of limited number of observations.A key example is that of the single latent variable simulation shown in Fig. 2B, where we could not reject a power law for the duration distribution.Conversely, strict application of the surrogate criteria would reject a power law for distributions that were quantitatively much closer to a power-law (i.e., lower KS statistic), but for which we had many more observations and thus a much stronger surrogate test (Fig. 2).This points to the difficulty of applying a single criterion to determining a power-law fit.In this work, we adhere to the criteria set forth in Clauset et al. (2009), with a modification to control for the unreasonably high statistical power of simulated data.Specifically, the number of avalanches used for fitting and for surrogate analysis was capped at 500, 000, drawn randomly from the entire pool of avalanches.
Additionally, we found examples, in which a short simulation was rejected, but increasing the simulation time by a factor of five yielded excellent power-law fits.We speculate that this arises due to insufficient sampling of the latent space.These observations raise an important biological point.Simulations provide the luxury of assuming the network is unchanging for as long as the simulator cares to keep drawing samples.In a biological network, this is not the case.Over the course of hours, the effective latent degrees of freedom could change drastically (e. g., due to circadian effects (Aton et al., 2009), changes in behavioral state (Fu et al., 2014), plasticity (Hooks and Chen, 2020), etc.), and the network itself (synaptic scaling, firing thresholds, etc.) could be plastic (Hengen et al., 2016).All of these factors can be modeled in our framework by determining appropriate cutoffs (in duration of recording, in time step sizes, for activity distributions) based on specific experimental timescales.

Calculation of avalanche regimes
In the quasistatic model, we derive the dependence of the avalanche rate on ,  and number of neurons , finding that there are two distinct regimes, in which avalanches occur.Each time bin is independent, conditioned on the value of ℎ.For an avalanche to occur, the probability of silence in the population (i.e., all   = 0) must not be too close to 0 (or there are no breaks in activity) or too close to 1 (or there is no activity).At fixed ℎ, the probability of silence is An avalanche occurs when a silent time bin is followed by an active bin, which has probability  ava (, ;   , , ℎ) =  silence (1 −  silence ).

Information calculation Maximum-likelihood decoding
For large populations coupled to a single latent variable, we estimated the information between population spiking activity and the latent variable as the information between the maximum-likelihood estimator ℎ * of the latent variable ℎ and the latent variable itself.This approximation fails at extremes of network activity levels (low or high).Specifically, we approximated the log-likelihood of ℎ * given ℎ true near ℎ * by log . Thus we assume that ℎ * is normally distributed about ℎ true with variance  2 (ℎ true ).The variance is then derived from the curvature of the log-likelihood at the maximum.The information between two Gaussian variables, here  (ℎ * |ℎ) = (ℎ,  2 ℎ * ) and (ℎ) = (0, 1), is where the average is taken over ℎ true ∼ (0, 1).Given a set of  observations of the neurons {  }, the likelihood is Maximizing the log likelihood gives the following condition: (18) To generate Figure 5, we evaluated Eqn. 10 using Eqn.18.We took a parameter combination with a low rate of avalanches but good apparent scaling ( = 4 and  = −14) and assumed that this is a reasonable estimate of the minimum number of observations (approximately 10 6 avalanches) required to observe scaling.To translate to observation length (in hours), we divided the number of avalanches observed in each full-length simulation by this minimum count and converted to a time using a time bin of 10 ms.Simulations were for a recorded population of 128 neurons.For this size of population,  0 = 5.2.

Figure 1 .
Figure 1.Latent dynamical variable model produces avalanche criticality.Simulated network is  = 1024 neurons.Other parameters in Table 1.A: Model structure.Latent dynamical variables ℎ  () are broadly coupled to neurons   () in the recorded population.B: Raster plot of a sample of activity binned at 3-ms resolution across 128 neurons with five latent variables, each with correlation timescale   = 15 s.C: Projection of activity into a simulated field of view for illustration.D-F: Avalanche analysis in a network (parameters   = 5,   = 10 4 ,  = 4 and  = 12), showing size distribution (D), duration distribution (E), and size with duration scaling (F).Lower cutoffs used in fitting are shown with vertical lines and their values are indicated in the figures.There are  obs = 42725 avalanches of size  ≥  min in this simulated dataset.Estimated values of the critical exponents are shown in the titles of the panels.

Figure 2 .
Figure 2. Multiple latent variables generate avalanche scaling at shorter timescales than a single latent variable.Simulated network is  = 1024 neurons.Other parameters used for simulations for this figure are found in Table 2. A-C: Scaling analysis for one variable models where the dynamic timescale is equal to 5 × 10 3 time steps.A: Distribution of avalanche sizes.MLE value of exponent for best-fit power law is  = 1.98 (0.02 SE), with lower cutoff indicated by the vertical line.B: Distribution of avalanche duration.MLE value of  is 1.81 (0.02 SE).C: Average size plotted against avalanche duration (blue points), with power-law fit (black line) and predicted relationship (yellow line) from MLE values for exponents in A and B. Gray bar on the horizontal axis indicates range, over which a power law with  = 1.72 fits the data (see Methods).D-F: Analysis of avalanches from a simulation of a population coupled to five independent latent variables where the dynamic timescale is equal to 5 × 10 3 time steps.G: Exponents  for avalanche size distributions across timescales for one-variable (blue) and five-variable (red) simulations.Each circle is a simulation with independently drawn coupling parameters.Simulations had to show scaling over at least two decades to be included in panels (G-J).H: Exponents  for avalanche duration distributions for simulations in G. I: Fitted values of  for simulations in G. J: Difference between fitted and predicted  values.Five-variable simulations produce crackling over a wider range of timescales than single-variable simulations.Figure 2-Figure supplement 1. Methods, power law distribution fits, one variable example.Figure 2-Figure supplement 2. Methods, power law distribution fits, five variable example.Figure 2-Figure supplement 3. Methods, gamma fit and range, one variable example.Figure 2-Figure supplement 4. Methods, gamma fit and range, five variables example.

Figure 2 -
Figure 2. Multiple latent variables generate avalanche scaling at shorter timescales than a single latent variable.Simulated network is  = 1024 neurons.Other parameters used for simulations for this figure are found in Table 2. A-C: Scaling analysis for one variable models where the dynamic timescale is equal to 5 × 10 3 time steps.A: Distribution of avalanche sizes.MLE value of exponent for best-fit power law is  = 1.98 (0.02 SE), with lower cutoff indicated by the vertical line.B: Distribution of avalanche duration.MLE value of  is 1.81 (0.02 SE).C: Average size plotted against avalanche duration (blue points), with power-law fit (black line) and predicted relationship (yellow line) from MLE values for exponents in A and B. Gray bar on the horizontal axis indicates range, over which a power law with  = 1.72 fits the data (see Methods).D-F: Analysis of avalanches from a simulation of a population coupled to five independent latent variables where the dynamic timescale is equal to 5 × 10 3 time steps.G: Exponents  for avalanche size distributions across timescales for one-variable (blue) and five-variable (red) simulations.Each circle is a simulation with independently drawn coupling parameters.Simulations had to show scaling over at least two decades to be included in panels (G-J).H: Exponents  for avalanche duration distributions for simulations in G. I: Fitted values of  for simulations in G. J: Difference between fitted and predicted  values.Five-variable simulations produce crackling over a wider range of timescales than single-variable simulations.Figure 2-Figure supplement 1. Methods, power law distribution fits, one variable example.Figure 2-Figure supplement 2. Methods, power law distribution fits, five variable example.Figure 2-Figure supplement 3. Methods, gamma fit and range, one variable example.Figure 2-Figure supplement 4. Methods, gamma fit and range, five variables example.

Figure 2 -
Figure 2. Multiple latent variables generate avalanche scaling at shorter timescales than a single latent variable.Simulated network is  = 1024 neurons.Other parameters used for simulations for this figure are found in Table 2. A-C: Scaling analysis for one variable models where the dynamic timescale is equal to 5 × 10 3 time steps.A: Distribution of avalanche sizes.MLE value of exponent for best-fit power law is  = 1.98 (0.02 SE), with lower cutoff indicated by the vertical line.B: Distribution of avalanche duration.MLE value of  is 1.81 (0.02 SE).C: Average size plotted against avalanche duration (blue points), with power-law fit (black line) and predicted relationship (yellow line) from MLE values for exponents in A and B. Gray bar on the horizontal axis indicates range, over which a power law with  = 1.72 fits the data (see Methods).D-F: Analysis of avalanches from a simulation of a population coupled to five independent latent variables where the dynamic timescale is equal to 5 × 10 3 time steps.G: Exponents  for avalanche size distributions across timescales for one-variable (blue) and five-variable (red) simulations.Each circle is a simulation with independently drawn coupling parameters.Simulations had to show scaling over at least two decades to be included in panels (G-J).H: Exponents  for avalanche duration distributions for simulations in G. I: Fitted values of  for simulations in G. J: Difference between fitted and predicted  values.Five-variable simulations produce crackling over a wider range of timescales than single-variable simulations.Figure 2-Figure supplement 1. Methods, power law distribution fits, one variable example.Figure 2-Figure supplement 2. Methods, power law distribution fits, five variable example.Figure 2-Figure supplement 3. Methods, gamma fit and range, one variable example.Figure 2-Figure supplement 4. Methods, gamma fit and range, five variables example.

Figure 2 -
Figure 2. Multiple latent variables generate avalanche scaling at shorter timescales than a single latent variable.Simulated network is  = 1024 neurons.Other parameters used for simulations for this figure are found in Table 2. A-C: Scaling analysis for one variable models where the dynamic timescale is equal to 5 × 10 3 time steps.A: Distribution of avalanche sizes.MLE value of exponent for best-fit power law is  = 1.98 (0.02 SE), with lower cutoff indicated by the vertical line.B: Distribution of avalanche duration.MLE value of  is 1.81 (0.02 SE).C: Average size plotted against avalanche duration (blue points), with power-law fit (black line) and predicted relationship (yellow line) from MLE values for exponents in A and B. Gray bar on the horizontal axis indicates range, over which a power law with  = 1.72 fits the data (see Methods).D-F: Analysis of avalanches from a simulation of a population coupled to five independent latent variables where the dynamic timescale is equal to 5 × 10 3 time steps.G: Exponents  for avalanche size distributions across timescales for one-variable (blue) and five-variable (red) simulations.Each circle is a simulation with independently drawn coupling parameters.Simulations had to show scaling over at least two decades to be included in panels (G-J).H: Exponents  for avalanche duration distributions for simulations in G. I: Fitted values of  for simulations in G. J: Difference between fitted and predicted  values.Five-variable simulations produce crackling over a wider range of timescales than single-variable simulations.Figure 2-Figure supplement 1. Methods, power law distribution fits, one variable example.Figure 2-Figure supplement 2. Methods, power law distribution fits, five variable example.Figure 2-Figure supplement 3. Methods, gamma fit and range, one variable example.Figure 2-Figure supplement 4. Methods, gamma fit and range, five variables example.

Figure 2 -
Figure 2. Multiple latent variables generate avalanche scaling at shorter timescales than a single latent variable.Simulated network is  = 1024 neurons.Other parameters used for simulations for this figure are found in Table 2. A-C: Scaling analysis for one variable models where the dynamic timescale is equal to 5 × 10 3 time steps.A: Distribution of avalanche sizes.MLE value of exponent for best-fit power law is  = 1.98 (0.02 SE), with lower cutoff indicated by the vertical line.B: Distribution of avalanche duration.MLE value of  is 1.81 (0.02 SE).C: Average size plotted against avalanche duration (blue points), with power-law fit (black line) and predicted relationship (yellow line) from MLE values for exponents in A and B. Gray bar on the horizontal axis indicates range, over which a power law with  = 1.72 fits the data (see Methods).D-F: Analysis of avalanches from a simulation of a population coupled to five independent latent variables where the dynamic timescale is equal to 5 × 10 3 time steps.G: Exponents  for avalanche size distributions across timescales for one-variable (blue) and five-variable (red) simulations.Each circle is a simulation with independently drawn coupling parameters.Simulations had to show scaling over at least two decades to be included in panels (G-J).H: Exponents  for avalanche duration distributions for simulations in G. I: Fitted values of  for simulations in G. J: Difference between fitted and predicted  values.Five-variable simulations produce crackling over a wider range of timescales than single-variable simulations.Figure 2-Figure supplement 1. Methods, power law distribution fits, one variable example.Figure 2-Figure supplement 2. Methods, power law distribution fits, five variable example.Figure 2-Figure supplement 3. Methods, gamma fit and range, one variable example.Figure 2-Figure supplement 4. Methods, gamma fit and range, five variables example.

Figure 3 .
Figure 3. Exponents across network simulations for networks of  = 128 neurons.Each parameter combination ,  was simulated for ten replicates, each time drawing randomly the couplings   , the latent variable values, and the neural activities.Other parameters in Table 3. A: Average across replicates for the size exponent .B: Scatter plot of  vs.  for each network replicate for parameter combinations indicated in A. Linear relationships between  and , corresponding to the minimum and maximum values of  f it from panel E, are shown to guide the eye.C: Same as A, for duration exponent .D: Predicted exponent,  pred , derived from A and C. E: Value of  f it from fit to S ∼   .F: Difference between  pred and  fit .

Figure 4 .
Figure 4. Avalanches in the latent dynamical variable model with a single quasistatic variable.Parameters in Table 3. A: Number of avalanches in simulations from Figure 3 as a function of the calculated probability of avalanches at fixed  across values of  and latent variable ℎ.Line indicates equality.B: Probability of avalanches with  = 2 across values of  and ℎ.The latent variable ℎ is normally distributed with mean 0 and variance 1.Where the distribution of ℎ overlaps with regions of high probability (black), avalanches occur.C: Probability of avalanches at  = 8 across values of  and ℎ.Increasing  narrows the range of ℎ that generates avalanches.D: Probability of avalanches at ℎ = 0 for a populations of 128 neurons (black line) and for a varying .Size distributions corresponding to simulations marked by the green and orange crosses are in E, F. E: Example of size distribution with  <  0 (orange marker in D).Size cutoff is close to 100.F: Example of size distribution with  >  0 (green marker in D).Size cutoff is < 10.

Figure 5 .
Figure 5. Information in the neural activity about the latent variable is higher in the low- avalanche region, compared to high- avalanche or high-rate avalanche-free activity.A: Probability of avalanche per time step across values of  and .Solid magenta curve follows  * (), the value of  maximizing the probability of avalanches at fixed .Dashed magenta line indicates  0 , calculated analytically, which matches  * at  = 0. B: Information about latent variable, calculated from maximum likelihood estimate of ℎ using population activity.MLE approximation is invalid in the dark-blue region bounded by gray curve.Magenta line marks the maximum values of  ava , reproduced from A. Dashed black curve indicates  ava = 0.001.The highest information region falls between  * () and the contour for  ava = 0.001.C -E: Slices of B, showing  MLE () for  = {2, 5, 9}.Magenta and dashed black lines again indicate  * and  ava = 0.001, respectively, as in B. Black dashed line marks the approximate boundary between the high-activity/no avalanche and the high-cutoff avalanche, and magenta line marks boundary between high-cutoff and low-cutoff avalanche regions.

Figure 2 -
Figure 2-Figure supplement 1. Illustration of algorithm for determining  and , using one variable example in Fig. 2. A-B: Probability density function for avalanche size (A) and duration (B) on a log-log scale, with the best power law fit (red).C-D: In blue: Maximum likelihood exponent of a power-law model as a function of the minimum (lower cutoff) size (C) and duration (D).In red: KS statistics (see Methods) for each fit."Best fit" is the power law with the minimum KS statistic.E-F: Surrogate data procedure.To generate each surrogate, samples were drawn from a power law with size / duration cutoff indicated (E,   = 3; F,   = 18) and the KS statistic was computed.Histograms illustrate KS statistic across surrogates (blue), while values derived from data are in red.Because the red line does not fall within the blue histogram, the hypothesis that the data is fitted well by a power law fit was rejected in E. At the same time, since the red line falls within the blue histogram in F, the hypothesis was accepted.

Figure 2 -
Figure 2-Figure supplement 2. Illustration of algorithm for determining  and , using example in Fig. 2, five latent variables.Notation the same as in Fig. 2-Fig.Supplement 3.

Figure 2 -
Figure 2-Figure supplement 3. Illustration of algorithm for fitting the exponent  and determining the range, over which power law scaling of average size with duration is observed, using example in Fig. 2(A-D).A-C: Determining the lower bound, the minimum duration   .A: The relation log  =  +  log  was fit using linear least-squares, restricted to (overlapping) 1-decade ranges (blue, red: example decades).B: Confidence intervals for fit parameters (,  for fits starting at each value of   .C: Best value of  min was selected based on how many subsequent start points yielded consistent slope/intercept values.D-F: Determining the upper bound, maximum duration   .D: Keeping   fixed based of value obtained in C, we test values of   up to the maximum duration event, and fit over the range [ min ,  max ].E: Average residual over the fit range [ min ,  min + 1], calculated for each fit and plotted against the value of  max used for that fit.The largest value of  max without evidence of bias in the residual was then selected.F: Final fit and range.

Figure 2 -
Figure 2-Figure supplement 4. Illustration of algorithm for fitting the exponent  and determining the range, over which power-law scaling of average size with duration is observed, using example in Fig. 2 E-H.See Fig. 2-Fig.Supplement 3 for caption.In this example, a lower value of  min was selected.Panel E, which was flat for Fig. 2-Fig.Supplement 3, now shows how extending the range to high values of  max can generate systematic errors at the low range of the fit, even while having a high overall goodness of fit metric.

Figure 4 -
Figure 4-Figure supplement 1.Estimate of how long it takes to observe avalanche criticality at each combination of  and .We took a parameter combination with a low rate of avalanches but good apparent scaling ( = 4 and  = −14) and assumed that this is a reasonable estimate of the minimum number of observations (approximately 10 6 avalanches) required to observe scaling.To translate to observation length (in hours), we divided the number of avalanches observed in each full-length simulation by this minimum count and converted to a time using a time bin of 10 ms.Simulations were for a recorded population of 128 neurons.For this size of population,  0 = 5.2.
ℎ −   ) − log(1 +  −(  ℎ+) )    is the average over observations .The uncertainty in ℎ * is  ℎ , which was calcu-lated from the second derivative of the log likelihood:This expression depends on the observations s only through the maximum-likelihood estimate ℎ * .When ℎ * → ℎ true , then the variance is